岩浆-流体过渡和阿尔泰三号伟晶岩脉之成因

本文对新疆阿尔泰可可托海的三号伟晶岩形成的物理化学条件、特别是流体-熔融包裹体进行了研究，证明岩浆的确可以分出热液，对于三号伟晶岩脉来说，这种热液组分主要是NaCl－CO2－H2O流体。     

南秦岭东江口、柞水岩体岩石谱系单位划分及演化

南秦岭东江口、柞水岩体位于南丹断裂带南侧,为华力西期岩基。通过1：5万地质填图,将东江口老体划分为5个岩石谱系单位,柞水岩体划分为3个岩石话系单位,共圈定出36个侵入体。分别建立了东江口超单元和排水超单元。依据接触关系,结构构造,包体特征确定了其侵入序次,构成了两个完整的“S”型岩浆演化序列,在岩石矿物组成、岩石化学成分、微量元素及稀土元素组成上,各具有明显的独特岩浆演化特征,分别形成于南秦岭晚古生代被动陆线构造环境。     

Pretreatment of high strength waste emulsions by combined vibratory shear enhanced process with Fenton oxidation

Pretreatment of waste emulsions with high organic content by a combined process of vibratory shear enhanced process and Fenton’s oxidation prior to biological treatment was investigated. Vibrating membrane had shown good performance in chemical oxygen demand and oil removals and the mitigation of concentration polarization. However, the permeate after filtration processing still contained high content of organics. Thus, additional Fenton oxidation was applied to reduce the organic loading, and improve the biodegradability of the wastewater. The optimal molar ratio of ferrous iron to hydrogen peroxide was 0.05 obtained from the jar-test experiments. Removal of organics was enhanced by increasing hydrogen peroxide dosage, while efficiency of hydrogen peroxide reached maximum of 1.11(w/w) at the hydrogen peroxide dosage of 6.8 g/L. Furthermore, the biological experiments indicated that the high concentration of organics could inhibit microbial activity, which decreased the chemical oxygen demand degradation rates. The adaptive period of the microbe was greatly shortened using Fenton’s reagent at the low dosages. The improvement of the biodegradability could be explained by partial mineralization and chemical transformation of parent organic compounds after Fenton oxidation.     

富氟花岗岩中萤石岩浆成因的新证据

通过富氟花岗岩-HF-H2O体系的熔化-结晶实验,在620～700℃、1×108Pa条件下获得了石英+碱性长石+黄玉+云母+萤石的矿物组合.在该实验体系中首次发现了八面体萤石.实验结果表明,在岩浆条件下可以形成萤石,从而为富氟花岗岩中萤石的岩浆成因提供了新证据.     

小体积萃取-石墨炉原子吸收法测定高纯硝酸钡中纳克级重金属元素

本文研究了石墨炉原子吸收光谱法测定高纯硝酸钡中超痕量重金属元素的分析技术。提出在大量钡基体存在时,采用小体积萃取体系APDC-MIBK同时萃取纳克级的Fe、Cu、Co和Ni。该法具有灵敏度高、无干扰、操作方便和减少沾污等特点。方法检出限为:Fe 7.2ng/g、Cu 12.8ng/g、Co 4.4ng/g和Ni 6.7ng/g。应用于红外光纤原料硝酸钡、硝酸铝中痕量重金属的测定,效果良好。     

长春黄土状土的水文、工程地质特性及降水方案的确定

在镜下对长春黄土状土的微观结构进行研究，发现第三层粉质粘土含水机制在于土中具有纵横交织的空洞和管道，地下水赋存于其中；第二层棕红色粉质粘土和粘土的崩解性在于该层土具有网状裂隙，卸荷后遇水崩解，在此基础上提出基坑降水的设计方案。     

Application research of narrow band Internet of things buoy and surface hydrodynamics monitoring

This paper applies the narrow band Internet of things communication technology to develop a wireless network equipment and communication system, which can quickly set up a network with a radius of 100 km on water surface. A disposable micro buoy based on narrow-band Internet of things and Beidou positioning function is also developed and used to collect surface hydrodynamic data online. In addition, a web-based public service platform is designed for the analysis and visualization of the data collected by buoys. Combined with the satellite remote sensing data, the study carries a series of marine experiments and studies such as sediment deposition tracking and garbage floating tracking.     

Li_2O-(Mg、Zn、Ni)O-V_2O_5三元体系的相平衡

对Li_2O-(Mg、Zn、Ni)O-V_2O_5三元体系在500—800℃相图的研究表明,在每个系统内部都出现了一个依端员组分摩尔比为1:2:1的化合物。即橄榄石型的LiMgVO_4,硅铍石型的LiZnVO_4和尖晶石型的LiNiVO_4。不同的是,Li_2O-MgO-V_2O_5中发现了第二个三元相和一个固溶体。LiO_2-NiO-V_2O_6中得出一个固溶体,而LiZnNO_4中未得固溶体。     

北京王四营地区土体旁压模量与压缩模量关系初探

城市化进程的加快,产生了人口密集、交通堵塞、资源短缺等诸多问题,城市空间需求增长与地面空间有限的矛盾日益突现,地下空间的开发利用越来越受到重视.北京交通网的建设已通过建设地铁线网、地下停车场和地下交通换乘枢纽形成地下交通系统,缓解了地面空间、环境资源对交通网的限制.以地下输送的高效率支持地下、地上各功能设施运转的高效率,局部地下空间利用已经超过50 m.为了使地下空间开发利用安全稳定,提供所需的岩土体物理力学参数(特别是50～100 m深度)具有重要的意义.北京王四营地区土体旁压试验,获取了0～100 m深度内黏性土及粉土力学性质,并在相同深度采取原状土样进行室内土工试验,分析了旁压模量和压缩模量随深度变化的相互关系,并用数理统计方法总结出二者的定量关系,为王四营地区100 m深度地下空间的利用提供可靠的力学参数.     

江汉盆地东部早中生代沉积地层碎屑云母成分:对大别高压-超高压岩石暴露作用的约束

碎屑白云母是碎屑岩中常见的、来自源区的稳定成分,可以用来指示源区性质,多硅白云母是碰撞造山高压-超高压变质岩石的特征矿物。对大别造山带同造山期沉积而成的江汉盆地东部上三叠统-中侏罗统砂岩碎屑白云母化学成分研究表明:上三叠统该区地层砂岩中碎屑白云母多以低硅白云母(Si<3.2)为特征,暗示此时大别造山带高压-超高压岩石很可能没有出露地表;自下侏罗统开始,砂岩中碎屑白云母中多硅白云母(Si>3.3)大量出现,中侏罗统砂岩多硅和低硅白云母发育,表明大别高压-超高压岩石在早侏罗世即已出露地表并经剥蚀搬运至盆地。这一结果从沉积学角度为约束高压-超高压岩石的折返时序和大别造山带演化提供了新的资料。